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Comparison of joint versus postprocessor approaches for hydrological uncertainty estimation accounting for error autocorrelation and heteroscedasticity

机译:联合方法和后处理器方法在水文不确定性估计中的比较,这些方法考虑了误差自相关和异方差性

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The paper appraises two approaches for the treatment of heteroscedasticity and autocorrelation in residual errors of hydrological models. Both approaches use weighted least squares (WLS), with heteroscedasticity modeled as a linear function of predicted flows and autocorrelation represented using an AR(1) process. In the first approach, heteroscedasticity and autocorrelation parameters are inferred jointly with hydrological model parameters. The second approach is a two-stage “postprocessor” scheme, where Stage 1 infers the hydrological parameters ignoring autocorrelation and Stage 2 conditionally infers the heteroscedasticity and autocorrelation parameters. These approaches are compared to a WLS scheme that ignores autocorrelation. Empirical analysis is carried out using daily data from 12 US catchments from the MOPEX set using two conceptual rainfall-runoff models, GR4J, and HBV. Under synthetic conditions, the postprocessor and joint approaches provide similar predictive performance, though the postprocessor approach tends to underestimate parameter uncertainty. However, the MOPEX results indicate that the joint approach can be nonrobust. In particular, when applied to GR4J, it often produces poor predictions due to strong multiway interactions between a hydrological water balance parameter and the error model parameters. The postprocessor approach is more robust precisely because it ignores these interactions. Practical benefits of accounting for error autocorrelation are demonstrated by analyzing streamflow predictions aggregated to a monthly scale (where ignoring daily-scale error autocorrelation leads to significantly underestimated predictive uncertainty), and by analyzing one-day-ahead predictions (where accounting for the error autocorrelation produces clearly higher precision and better tracking of observed data). Including autocorrelation into the residual error model also significantly affects calibrated parameter values and uncertainty estimates. The paper concludes with a summary of outstanding challenges in residual error modeling, particularly in ephemeral catchments.
机译:本文评估了两种处理水文模型残差中的异方差和自相关的方法。两种方法都使用加权最小二乘(WLS),将异方差建模为预测流量和使用AR(1)流程表示的自相关的线性函数。在第一种方法中,与水文模型参数一起推断异方差和自相关参数。第二种方法是两阶段的“后处理器”方案,其中阶段1忽略自相关而推断水文参数,阶段2有条件地推断异方差性和自相关参数。将这些方法与忽略自相关的WLS方案进行了比较。使用来自MOPEX集的12个美国集水区的每日数据,使用两个概念性降雨径流模型GR4J和HBV,进行了实证分析。在综合条件下,尽管后处理器方法倾向于低估参数不确定性,但后处理器方法和联合方法可提供相似的预测性能。但是,MOPEX结果表明联合方法可能不可靠。特别是,当将其应用于GR4J时,由于水文水平衡参数与误差模型参数之间存在很强的多路交互作用,因此常常产生较差的预测。后处理器方法更加健壮,因为它忽略了这些交互。通过分析汇总到月度尺度的流量预测(忽略每日尺度的误差自相关会导致大大低估了预测不确定性),以及通过分析提前一天的预测(其中考虑了误差自相关),说明了误差自相关的实际好处。产生明显更高的精度并更好地跟踪观察到的数据)。将自相关包括在残差模型中,也会显着影响校准后的参数值和不确定性估计。本文最后总结了残留误差建模中的突出挑战,特别是在临时流域。

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